Dynamic Phase Alignment in Inertial Alfv´en Turbulence

ORAL

Abstract

In weakly-collisional plasma environments with sufficiently low electron beta, Alfv\'enic turbulence transforms into inertial Alfv\'enic turbulence at scales below the electron skin-depth, $k_\perp d_e > 1$. We argue that, in inertial Alfv\'enic turbulence, both energy and generalized kinetic helicity exhibit direct cascades. We demonstrate that the two cascades are compatible due to the existence of a strong scale-dependence of the phase alignment angle between velocity and magnetic field fluctuations, with the phase alignment angle scaling as $\cos\alpha_k\propto k_{\perp}^{-1}$. As a result of the dual direct cascade, the generalized-helicity spectrum scales as $\propto k^{-5/3}_{\perp}$, implying progressive balancing of the turbulence as the cascade proceeds to smaller scales in the $k_{\perp} d_e \gg 1$ range. Our results may be applicable to a variety of geophysical, space, and astrophysical environments, including the Earth's magnetosheath and ionosphere, solar corona, non-relativistic pair plasmas, as well as to strongly rotating non-ionized fluids.

* L.M.M. was supported by the DoE grant No. DE-FG02-91ER54109. N.F.L. was partly funded by the NSF CAREER award No. 1654168 and by the Prof. Amar G. Bose Research Fellows Program at MIT. S.B. was partly supported by the NSF grant No. PHY-1707272, NASA grant No. 80NSSC18K0646, and DOE grant No. DESC0018266.

Authors

  • Lucio Milanese

    Massachusetts Institute of Technology

  • Nuno Loureiro

    Massachusetts Institute of Technology

  • Maximilian Daschner

    ETH Zurich and Massachusetts Institute of Technology

  • Stanislav Boldyrev

    University of Wisconsin - Madison, Department of Physics, University of Wisconsin - Madison, University of Wisconsin-Madison